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An island, or in the case of very large ones, a continental landmass.
hat there was once a supercontinent and the huge landmass was broken into continents that drifted apart .
Continental drift is the idea that Wegener created, that all the continents were once a single landmass which he called Pangaea, and they have since drifted apart.
They are spread apart now because before the were one big landmass.
The continental shelf is the term for part of a continent that extends outward from the landmass beneath shallow seawater. The drop-off point of a continental shelf is called the shelf break. From this point, the continental goes down to the deep ocean floor.
Antarctica
the answer to the question is: continental slope
Geologists study the movements of continental landmasses through the field of plate tectonics. They investigate how the Earth's lithosphere is broken into plates that move over the semi-fluid asthenosphere, leading to phenomena such as earthquakes, mountain building, and the formation of ocean basins.
The continental shelf edge is an area that is located at the edge of an underwater landmass. This landmass extends out from a continent and has a relatively shallow area of water which is often referred to as the shelf sea.
Europe is not on an island. It is part of the continental landmass known as Eurasia.
Europe is not on an island. It is part of the continental landmass known as Eurasia.
a continental theory
This idea is called the theory of continental drift, which suggests that all continents were once part of a single landmass called Pangaea that later split and drifted apart over millions of years.
Alfred wegener came up with the theory of continental drift, when all of the continents were together as one the landmass was called Pangea
No. It is joined to Asia, forming a continental landmass known as Eurasia.
continental drift :D
The continental shelves were formed millions of years ago, when most of the land on the Earth was compacted into one huge landmass. After some time, this landmass began to break into smaller pieces, which became the continental shelves. Then they drifted farther and farther apart and appear where they are today.